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Dryad

Data from: Ocean circulation changes rather than global warming drove temperature trends across the Miocene Climatic Optimum

Abstract

The Early-to-Middle Miocene (23-13.8 million years ago, Ma) was 6–9 °C warmer than today. Around 16.9 Ma, benthic foraminiferal oxygen isotope (d18O) records suggest pronounced warming, known as the Miocene Climate Optimum (MCO) onset. However, explaining this putative global warming with CO2 forcing faces challenges in terms of timing and forcing magnitude. Our new biomarker-based ocean temperature records, combined with published data, reveal no significant mean global upper ocean warming across the MCO. Instead, temperature changes differ considerably between sites, with some regions showing cooling. Climate model sensitivity tests indicate these patterns are best explained by ocean circulation changes, likely due to gateway changes and Antarctic ice sheet variations. This suggests that the MCO signature is better attributed to ocean circulation changes rather than a CO2-driven global warming event. The d18O signal therefore represents warmer deepwater sourcing and/or reduced Antarctic glacial volume, resolving the longstanding challenge of explaining MCO warming without a pronounced CO2 rise.